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MEASUREMENT OF INTENSITY OF LIQUID PRECIPITATION USING DOUBLEFREQUENCY RADAR

机译:双重雷达测量液体降水强度

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The rain intensity is very important characteristic of precipitation which is useful for many fields of people activity, especially for such areas as agriculture and municipal services. That is why it is of big interest now to develop new approaches to measure precipitation intensity the most popular of which is radar methods permitted to obtain data distantly and promptly for large territories. Now it is known some radar approaches for measurement of rain precipitation. But the method grounded on measurement of radar reflectance Z mm6/m3 is the most widespread. It is based on use of dependence- Z=x/y, where x and y - some constants, depended on climatic, geographic conditions and mechanism. of precipitation formation. The inain disadvantage of such approach-is absence of universal correlation between radar reflectance and rain intensity. Accordingly data of different authors [1,2] the values of parameter x man be varied from 50 to 2000, y-from 1 to 2,87. Such variation of parameters x and y strongly influences on accuracy of intensity measurement.
机译:雨强度是沉淀的非常重要的特征,这对于许多人的活动有用,特别是对于农业和市政服务的区域。这就是为什么它现在具有大兴趣的原因,以衡量降水强度的新方法,最受欢迎的是,最受允许的雷达方法,允许为大型地区远端和及时获得数据。现在已知一些用于测量雨水降水的雷达方法。但是在雷达反射率测量上接地的方法是最普遍的ZM6 / M3。它基于使用依赖性 - z = x / y,其中x和y - 一些常数,取决于气候,地理条件和机制。沉淀形成。这种方法的缺点 - 没有雷达反射率和雨强度之间的通用相关性。因此,不同作者的数据[1,2]参数x人的值从50到2000,y-y-y-y-y-u到2,87变化。参数X和Y的这种变化强烈影响强度测量的准确性。

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